% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 14 % Primary Name: SOVIETSKAYA % Record Type: TAVG % Country: Antarctica % Latitude: -78.40000 +/- 0.05000 % Longitude: 87.60000 +/- 0.05000 % Elevation (m): 3570.00 +/- 0.50 % # of Months: 10 % % IDs: wmssc - 895570 % % Sources: World Monthly Surface Station Climatology % % Site Hash: b77a6c8f6571c35a51e0effd24e3fa73 % Raw Data Hash: fb2ab01328364a863b7b3e71e7cdad3e % Adj Data Hash: fb2ab01328364a863b7b3e71e7cdad3e % % The data for this station is presented below in several columns and in % several forms. The temperature values are reported as "raw", % "adjusted", and "regional expectation". % % The "raw" values reflect the observations as originally ingested by % the Berkeley Earth system from one or more originating archive(s). % These "raw" values may reflect the merger of more than one temperature % time series if multiple archives reported values for this location. % Alongside the raw data we have also provided a flag indicating which % values failed initial quality control checks. A further column % dates at which the raw data may be subject to continuity "breaks" % due to documented station moves (denoted "1"), prolonged measurement % gaps (denoted "2"), documented time of observation changes (denoted "3") % and other empirically determined inhomogeneities (denoted "4"). % % In many cases, raw temperature data contains a number of artifacts, % caused by issues such as typographical errors, instrumentation changes, % station moves, and urban or agricultural development near the station. % The Berkeley Earth analysis process attempts to identify and estimate % the impact of various kinds of data quality problems by comparing each % time series to neighboring series. At the end of the analysis process, % the "adjusted" data is created as an estimate of what the weather at % this location might have looked like after removing apparent biases. % This "adjusted" data will generally to be free from quality control % issues and be regionally homogeneous. Some users may find this % "adjusted" data that attempts to remove apparent biases more % suitable for their needs, while other users may prefer to work % with raw values. % % Lastly, we have provided a "regional expectation" time series, based % on the Berkeley Earth expected temperatures in the neighborhood of the % station. This incorporates information from as many weather stations as % are available for the local region surrounding this location. Note % that the regional expectation may be a systematically a bit warmer or % colder than the weather stations by a few degrees due to differences % in mean elevation and other local characteristics. % % For each temperature time series, we have also included an "anomaly" % time series that removes both the seasonality and the long-term mean. % These anomalies may provide an easier way of seeing changes through % time. % % Reported temperatures are in Celsius and reflect monthly averages. As % these files are intended to be summaries for convenience, additional % information, including more detailed flagging and metadata, may be % available in our whole data set files. % % The Berkeley Earth analysis was run on 15-Nov-2013 19:55:48 % % Raw Data QC Continuity Adjusted Data Regional Expectation % Year, Month, Temperature, Anomaly, Failed, Breaks, Temperature, Anomaly, Temperature, Anomaly 1957 3 NaN NaN NaN NaN NaN NaN -51.880 0.463 1957 4 NaN NaN NaN NaN NaN NaN -51.669 6.251 1957 5 NaN NaN NaN NaN NaN NaN -58.983 1.421 1957 6 NaN NaN NaN NaN NaN NaN -54.474 6.040 1957 7 NaN NaN NaN NaN NaN NaN -60.413 1.570 1957 8 NaN NaN NaN NaN NaN NaN -56.966 5.171 1957 9 NaN NaN NaN NaN NaN NaN -56.557 4.120 1957 10 NaN NaN NaN NaN NaN NaN -49.189 4.509 1957 11 NaN NaN NaN NaN NaN NaN -39.867 1.605 1957 12 NaN NaN NaN NaN NaN NaN -32.519 -0.040 1958 1 NaN NaN NaN NaN NaN NaN -32.212 0.753 1958 2 NaN NaN NaN NaN NaN NaN -43.785 -1.445 1958 3 -54.300 3.009 0 0 -54.300 3.009 -50.252 2.091 1958 4 -60.400 2.487 0 0 -60.400 2.487 -55.708 2.212 1958 5 -67.300 -1.929 0 0 -67.300 -1.929 -60.332 0.072 1958 6 -69.500 -4.020 0 0 -69.500 -4.020 -63.460 -2.946 1958 7 -69.500 -2.550 0 0 -69.500 -2.550 -62.686 -0.703 1958 8 -71.900 -4.796 0 0 -71.900 -4.796 -65.698 -3.561 1958 9 -66.700 -1.056 0 0 -66.700 -1.056 -61.142 -0.465 1958 10 -59.700 -1.035 0 0 -59.700 -1.035 -54.817 -1.118 1958 11 -43.300 3.139 0 0 -43.300 3.139 -40.383 1.090 1958 12 -33.400 4.046 0 0 -33.400 4.046 -31.857 0.622 1959 1 NaN NaN NaN NaN NaN NaN -34.510 -1.545 1959 2 NaN NaN NaN NaN NaN NaN -41.818 0.521 1959 3 NaN NaN NaN NaN NaN NaN -49.461 2.882 1959 4 NaN NaN NaN NaN NaN NaN -55.554 2.366 1959 5 NaN NaN NaN NaN NaN NaN -59.073 1.331 1959 6 NaN NaN NaN NaN NaN NaN -61.220 -0.706 1959 7 NaN NaN NaN NaN NaN NaN -62.988 -1.005 1959 8 NaN NaN NaN NaN NaN NaN -62.368 -0.230 1959 9 NaN NaN NaN NaN NaN NaN -63.890 -3.213 1959 10 NaN NaN NaN NaN NaN NaN -53.504 0.195 1959 11 NaN NaN NaN NaN NaN NaN -42.332 -0.859 1959 12 NaN NaN NaN NaN NaN NaN -31.695 0.785